For aviation and nautical navigation, the wind triangle is very important for determining the relations between the course and heading. Here, the general wind triangle is solved with an aviation flavor.
The wind triangle can be solved via permutations of the two governing geometric relationships derived from the Law of Sines and Law of Cosines (notation is explained in later):
sin(Φ−Ψ)G=sin(Θ−Ψ)V=sin(Θ−Φ)W
G2=V2+W2−2VWcos(Φ−Ψ)
These equations hold for the domain of angles between 0∘≤∠≤360∘. These equations assume that the wind speed are approximately less than 20% of the true air speed. They work at higher ratios with one caveat.
The wind triangle is generally used to solve 1 of 3 different problems, two of which is considered the "direct" problem and the last being the "inverse" problem. Nihad E. Daidzic 2016
Direct Problems:
The airspeed, heading, wind direction, and wind speed are known; the ground speed, drift angle, and the true course are calculated. (This problem shall be called the secondary direct problem.)
The airspeed, true course, wind direction, and wind speed are known; the ground speed, wind correction angle, and required heading are calculated. (This problem shall be called the primary direct problem.)
Inverse Problem:
The airspeed, ground speed, heading, and course are known. The wind direction and wind speed are calculated. (This problem shall be called the primary inverse problem.)
The solutions to these problems in generalized mathematical form are provided.
We will use the following wind triangle as a visual and notional reference along with the following notation: (For the sake of the equations often found on a E6B, Φ=Θ−L+R∇, the drift angle is Δ and the wind correction angle is ∇.)
(Only the physically important angles are listed.)
Three separate geometric and trigonometric identities are needed. Consider a triangle with the following general dimensions:
Euclidean triangles such as these follow these properties:
Triangle Postulate The sum of all angles of the triangle is equal to two right angles. Thus:
a+b+c=2(2π rad)=π rad=180∘
Law of Sines The ratio of sides and the sines of their opposite angles are equal. Thus:
sinaA=sinbB=sincC
Law of Cosines The Pythagorean theorem extended for any triangle that is not a right triangle. Thus:
C2=A2+B2−2ABcosc
Two other miscellaneous geometric properties are needed.
Supplementary Angles A linear pair of angles (two angles which share only one side and their non-shared sides are the same line) sum to a straight angle ∠=180∘=π rad.
Conjugate Angles A pair of non-congruent angles which share the same sides sum to a complete angle ∠=360∘=2π rad.
Often E6Bs are used for the quick slide-rule calculations of many of these values here. For these calculations, we use the drift angle Δ defined by: (For the course Θ and the heading Φ.)
Δ=Θ−Φ
But, E6Bs have the notation: (Here, notationally, the wind correctional angle is given as ∇.)
MH=MC−L+RWCA⟶Φ=Θ−L+R∇=Θ±∇
Conventionally, it is assumed that Δ=−∇. However, this is only the case for where wind speed to airspeed ratio r≜VW⪅0.2, the deviation being on the order of ∠≲1∘ (Alexander W S et. al. 1941). That is assumed here, as such:
∇=−Δ
Should these equations be used in the domain of r≜VW≈0.2, corrections to the current course may need to be done more frequently to fix the small deviation.
Here we present the general solutions to the different types of problems initally described, provided the governing equations found above.
Note, generally, the Law of Cosines is more numerically stable to rounding errors than the Law of Sines. It also does not suffer from the Law of Sines ambiguity.